HR: 0800h
AN: S21B-0572 [Abstracts]
TI: Dynamic Slip in 2D Discrete Element Method Numerical Simulations of a Rough Fault
AU: Abe, S
EM: s.abe@ged.rwth-aachen.de
AF: Seismology and Computational Rock Physics Lab, School of Geological Sciences,
University College Dublin, Belfield, Dublin, 4, Ireland
AU: * Bean, C J
EM: chris.bean@ucd.ie
AF: Seismology and Computational Rock Physics Lab, School of Geological Sciences,
University College Dublin, Belfield, Dublin, 4, Ireland
AB:
2D discrete element method (DEM) simulations are used to investigate the properties of the dynamic rupture of a
heterogeneous fault. The model consists of two rectangular blocks of fully bonded particles with a pre-existing
fault between the blocks across which the particles are not bonded and interact only by frictional forces. An
intrinsic small scale roughness of the fault surface is present due to the construction of the fault model from
random spherical particles. Additionally, heterogeneity on a large length scale is introduced, generating asperity
and non-asperity regions along the fault by varying the amount of small-scale surface roughness between these
regions. Contact friction is defined using a Coulomb Law.
The model evolves from a stress-free initial state into stick-slip behaviour while a constant normal stress and a
constant shear velocity are applied to the edges of the model.
The resulting slip events show a number of properties similar to real seismic events. We observe qualitatively
realistic source-time functions, although the absolute slip velocities are too high, realistic stress drops and
rupture velocities. The power spectral density (PSD) of the resulting slip distributions is consistent with a fractal
distribution, as observed in nature. The results indicate that a simple friction law coupled with geometrical
complexity yields many of the characteristic features seen in real rupture propagation.
DE: 7209 Earthquake dynamics (1242)
DE: 7290 Computational seismology
DE: 8118 Dynamics and mechanics of faulting (8004)
SC: Seismology [S]
MN: 2007 Fall Meeting